摘要
本文用五个地磁台站的静日日变资料重新研究中国东南地区的深部电导率分布。这五个台站是:武汉、佘山、广州、泉州与仑坪。五台定出的C值结果与文献〔1〕的不同。另外本文用简单的蒙特卡罗(Monte-Carlo)法反演推断可能的电性结构模型。
The quiet daily magnetic variation data of five observatories, Wuhan, Sheshan, Guangzhou, Quanzhou and Lunping, were vised for studying the deep electrical conductivity structure beneath the region of southeast China. The results of the C-value are different from that obtained in Reference [1]. Besides, a simple Monte-Carlo inversion procedure is applied to the C-value data in this paper for deducing the acceptable interpretation of the electrical conductivity structure.
出处
《地震研究》
CSCD
北大核心
1989年第4期348-352,共5页
Journal of Seismological Research
关键词
电导率
电性结构模型
东南地区
southeast China, electrical conductivity, electrical conductivity structure model
